SAI Platform
June 2010
This document has been produced for internal information purposes only among SAI platform members. It represents a collection of information that is freely available on the internet, and that we believe to be accurate. Nevertheless, it is by no means an exhaustive document and no guarantee is provided about the content. The views expressed herein do not reflect the official opinion of SAI platform, nor its members.
WATER CONSERVATION
TECHNICAL BRIEFS
TB5 - The Importance of Soil to Water Use
TB 5 – The Importance of Soil to water use
1
WATER CONSERVATION
TECHNICAL BRIEFS
TB5 - The Importance of Soil to Water Use
Soil properties strongly influence water storage and availability. A comprehensive
understanding of the movement of water in soil can help understanding how much
water the soil holds, the movement of water in soils assessing irrigation practices and
designing an adequate irrigation system. This technical brief aims at describing how soils
hold water and identifying soil moisture monitoring tools and methods. This brief is
intended to be an introduction to irrigation scheduling.
The structure of the technical brief is as follows: Section 1 explains the size and
arrangement of soil particles and pores influences water movement in soil. Sections 2
and 3 provide an explanation of soil properties: texture and structure respectively.
Section 4 outlines the water movement in soil such as infiltration, runoff and capillarity.
Section 5 presents how soil can be sampled to determine soil moisture levels. Section 6
describes soil moisture. Section 7 introduces briefly how to schedule irrigation by
measuring soil moisture. Section 8 presents technical soil moisture monitoring
equipment available for farmers to monitor water use. Section 9 suggests how to
interpret data from the monitoring equipment. Section 10 illustrates a case study of use
of tensiometres to assess soil moisture to grow tomatoes. Finally, Section 11
recommends some further reading.
TB 5 – The Importance of Soil to water use
2
Contents Section 1: How soil influences water use? ......................................................................... 3
Section 2: What is soil texture? .......................................................................................... 3
Section 3: What is soil structure? ....................................................................................... 5
Section 4: Movement of water in soil ................................................................................. 6
a. Water infiltration ..................................................................................................... 6
b. Runoff ....................................................................................................................... 6
c. Capilarity .................................................................................................................. 7
Section 5: Soil sampling ...................................................................................................... 7
Section 6: Soil moisture levels ............................................................................................ 8
a. Readily Available Water (RAW)................................................................................ 8
b. Refill point ................................................................................................................ 9
c. Permanent wilting point .......................................................................................... 9
d. Gravitational water .................................................................................................. 9
e. Field capacity ........................................................................................................... 9
Section 7: When to irrigate? ............................................................................................. 10
Section 8: How to measure soil moisture? ....................................................................... 11
a. Soil Suction Measurement Systems ....................................................................... 11
b. Soil Moisture Content Measurement Systems ...................................................... 12
Section 9: How to interpret soil moisture data? .............................................................. 14
Section 10: Case Study ...................................................................................................... 16
Section 11: References and further readings ................................................................... 18
TB 5 – The Importance of Soil to water use
3
SECTION 1: HOW SOIL INFLUENCES WATER USE? Soil management is linked to water use as soil properties
influence the movement and storage of water. Soil texture
and soil structure, strongly influence the way water behaves
in a soil. Moreover, these properties affect the movement
of water into the soil, drainage and water storage in the soil
profile.
The reason that texture and structure have such a strong
influence on water storage and availability is the size of soil
particles and pores, and their arrangement. The soil texture
determines the capacity of the soil of holding water. A soil
with large particles and large pore spaces (e.g. sand) hold
the least amount of water. On the other hand, a soil rich in
clay has small particles and can store a large amount of
water. However, not all of it is available to plants as small
pores hold onto water very tightly. Compacted soil has
small, disconnected pore space which reduces the amount
of water that is available to plants. Figure 1 depicts a soil
profile where different types of soil can be distinguished.
By understanding how soil properties affect water storage before designing an adequate
irrigation system can help optimising water use by plants.
SECTION 2: WHAT IS SOIL TEXTURE?1
Soil texture is the amount of sand, silt and clay in the
soil. It has a strong influence on water storage and
availability because of the variation in the particle size
distribution and the surface area. Figure 2 shows the
different textures of soil depending on its percentage of
sand, silt and clay.a Clay particles are small (diameter <
0.002mm) compared to larger sand particles (diameter
a To see an enlarger version of the figure visit soils.usda.gov/
Figure 2: Percentage of clay, silt and sand in the basic soil textural classes.
Figure 2
Figure 1: Soil profile
TB 5 – The Importance of Soil to water use
4
between 0.02 – 2 mm). Smaller particles fit together more tightly than larger particles
and therefore the pores for air and water are also smaller. Small pores retain water
against gravitational forces, drainage and also against plant use, while the larger pores
found in sand allow water to drain.
Ideally, a soil will contain a range of pore sizes, larger pores which drain readily so as to
prevent water logging following soil saturation and smaller pores which store water for
plant use. Not all water held in very small pores is available to plants because water can
be retained strongly.b
The amount of water that can be absorbed by the soil increases as the surface area of
the particles in the soil increases. Fine clay has about 10,000 times as much surface area
as the same weight of medium-sized sand. Soil with high organic matter can also retain
water very well.
Soil texture can be determined in farm by the way the soil behaves when a small
amount of soil is moistened and pressed out between the thumb and forefinger to form
a ribbon. Figure 3 shows a methodology used when determining the texture of a soil in
farm.c
b Of most importance for plant growth is the amount of water stored in the soil that is readily available for
uptake by plants rather than the total amount of water stored in the soil profile. The water that plants can
easily remove from the soil is called Readily Available Water (RAW). c An enlarged version of the figure can be found at http://attra.ncat.org/attra-pub/soil_moisture.html
TB 5 – The Importance of Soil to water use
5
Section 3: What is soil structure?
Soil structure is the arrangement of the solid components of soil and the spaces in
between. Ideally, soil should have pores for the flow of water and gases, and pores that
contain water and dissolved nutrients for plant
growth.d
Plants grow best when they have a suitable
balance of water and air in their root zones. The
soil within the root zone needs to be able to
store as much water as possible in the plant
available range but also needs to be able to
drain enough water so that aeration is quickly
re-established after irrigation and/or rainfall.
To maintain a good structural form some
measures can be taken. Some of them are to
improve organic matter content, to encourage
soil fauna such as earthworms and to avoid
cultivation when it is too dry. When a soil is
badly compacted structural form needs to be
firstly regenerated using biological solutions
(e.g. rotation crops) and appropriate tillage
methods.e
d A soil is badly compacted if the pore space is reduced so the water transmission through the soil is
slowed and water storage and aeration is minimised. A surface crust increases runoff, which reduces the
efficiency of rainfall and irrigations. A compacted soil will have reduced readily available water (RAW),
compared to a soil with the same texture but with better structural form. A reduction of RAW can cause a
moisture stress on a compacted soil even if there is sufficient rainfall and irrigation, because of a
reduction in RAW. Root growth is also impeded in a compacted soil and they are not able to harvest water
from as large an area as would be possible if their growth was not restricted.
e See technical Brief on Conservation Tillage for further information.
Figure 3: Methodology to assess soil texture in farm.
TB 5 – The Importance of Soil to water use
6
SECTION 4: MOVEMENT OF WATER IN SOIL
a. Water infiltration
A function of soil is to absorb water at the land surface, and store it for use by plants or
slowly release it to groundwater through gravitational flow. When rainfall hits the
ground, most water will infiltrate the soil; but some may run off the surface, and some
may stand in ruts or depressions before infiltrating or evaporating.
The infiltration capacity is the maximum amount of rainwater that can enter a soil in a
specific time. It is influenced by the soil type, structure, and moisture content at the
start of the rain.
Sandy and gravelly soils have more large pores than fine loams and clays, and therefore
they maintain better infiltration during a storm. But soil texture influences the number
of pores and their sizes: When finer-textured soils have strong aggregates due to good
management, they can also maintain high infiltration rates.
Soil compaction can reduce the infiltration rate. Soil compaction occurs when soil
particles are pressed together, reducing pore space. Heavily compacted soils contain
few large pores and have a reduced rate of both water infiltration and drainage from
the compacted layer. This occurs because large pores are the most effective in moving
water through the soil when it is saturated.2
There are several forces, natural and man-induced, that compact a soil. This force can
be great, such as from a tractor, combine or tillage implement, or it can come from
something as small as a raindrop.f
A compacted soil can be repaired using a workable combination of break and rotation
crops that provide natural crop-induced wetting and drying cycles to crack the soil; root
penetration to break up massive and platy soil structure; increased organic matter to
enrich and strengthen the soil.3
b. Runoff
When rainfall exceeds the soil’s infiltration capacity, runoff is produced. Rainfall or
snowmelt on frozen ground generally poses even greater runoff concerns, as pores are
blocked with ice. Runoff happens more readily with poorly managed soils, because they
f For more information on how to reduce ploughing see Technical Brief on Conservation Tillage.
TB 5 – The Importance of Soil to water use
7
lack strong aggregates that hold together against the force of raindrops and moving
water and, therefore, have few large pores open to the surface to quickly conduct water
downward. Such runoff can initiate erosion, with losses of nutrients and agrochemicals
as well as sediment. Runoff directly depends on the rainfall and raindrop impact on soil,
the soil erodibility which is based on soil properties, slope gradient and extent, soil
cover and conservation practices.4
c. Capilarity
Capilarity rise is the process where groundwater is sucked upward by the soil through
very small pores that are called capillars. The movement of the water depends on soil
texture; in clay soils the upward movement of water is slow but covers a long distance.
In sandy soils, the upward movement of the water is quick but covers only a short
distance.5
SECTION 5: SOIL SAMPLING6
Soil sampling is commonly used to determine the amount of soil moisture. The wetness
of the soil can be described as the gravimetric soil water content, the volumetric soil
water content and the soil water potential (also known as soil water suction).
• Gravimetric soil water content: is the quantity of water in the soil on a weight
basis. It is expressed on gr of water per gr of dry soil)
• Volumetric soil water content: is the quantity of water on a volumetric fraction
of soil. It is measured by calculating the quantity of water per unit of soil and
multiply it by the soil bulk density. It is expressed in ccg of water per cc of soil.
• Soil water potential or soil water suction: is the pressure needed to extract
water from the soil. This measure is used because some soils hold water more
tightly than others, and all soils hold water more tightly as they dry. It represents
the energy plants must exert to draw water from the soil. Soil water suction can
be measured by porous media (e.g. gypsum blocks) or wetting front detectors
(e.g. FullStop), which are devices that detect when water moves down through
the soil to them. The soil water potential is expressed in kilopascals (kPa).
g cubic centimetres
TB 5 – The Importance of Soil to water use
8
SECTION 6: SOIL MOISTURE LEVELS Soil texture and structure information can be used to estimate soil water holding
capacity, which in turn is used in planning irrigation design and operation. Ideally, the
soil condition should be assessed before a new field is developed for vegetable
production so that the irrigation design can be matched to the soil types in the farm. If
this is not done then some areas can be over-watered, while others will not be watered
enough. The amount of water to be applied per irrigation event, and the time between
irrigation events will vary between soil types.
Figure 4 below shows the percentage of soil moisture levels over time for a specific
crop. As shown in the picture, the soil moisture varies from saturation to permanent
wilting point. This diagram helps to understand when the crops require water. Some
useful concepts depicted on the figure 4 are described below.
Figure 4. Soil Moisture over time7
a. Readily Available Water (RAW)8
In simple terms, the Readily Available Water (RAW) is the water that a plant can easily
extract from the soil. RAW is the soil moisture held between field capacity and a
nominated refill point for unrestricted growth. In this range of soil moisture, the plants
have good condition to grow and are neither waterlogged nor water-stressed.
TB 5 – The Importance of Soil to water use
9
The RAW can be calculated by multiply the thickness of each soil layer (in centimetres)
by the RAW of that layerh. Then add the values for each soil layer in the root zone to get
the total root zonei RAW.
b. Refill point
As water is removed by plants and by evaporation from the soil surface it becomes more
and more difficult for plants to extract water as it clings more tightly to soil particles and
in small pore spaces. When water extraction becomes difficult for plants and more
water is required to maintain growth rates, the soil is said to be at the ‘refill point’. If the
soil dries to the permanent wilting point, the plant can no longer remove any water
from it. The drier the soil, as shown by high tensiometer values, the more water needs
to be added to bring the soil back to field capacity. Refill point for horticultural crops lies
between a tension of -20 and -60 kPa.
c. Permanent wilting point
Eventually, if the soil continues to dry, it will hold some water which cannot be
extracted by plant roots and plants wilt and cannot recover. This is called the Permanent
Wilting Point (PWP). Plant production will slow/stop before PWP is reached (a tension of
-1500 kPa).
d. Gravitational water
As water infiltrates the soil, it fills the pore spaces between the soil particles.
Gravitational water is the status when pores are completely saturated and therefore
water percolates down through the soil profile and below the root zone. Gravitational
water may take a few hours to drain away in sandy soils, or days or even weeks in clay
soils (See figure 5 below).
e. Field capacity
Field capacity is the condition of equilibrium when the gravity forces are equal to the
evaporation forces. Evaporation at the soil surface pulls water upward through capillary
h The RAW properties are fixed values that depend on the texture of the soil and vary according to the
area. i Plants get most of their water from the upper (shallow) portion of the root zone. The term effective root
zone refers to about the upper half of the root zone depth, where roughly 70 percent of the plant’s water
is taken up.
TB 5 – The Importance of Soil to water use
10
forces, while capillary forces also hold water around the soil particles. In this condition,
water stops moving downward and is held by surface tension in the soil. (See figure 5)
SECTION 7: WHEN TO IRRIGATE?j Irrigation should occur before soil moisture depletion reduces crop yields. Two
approaches for determining when to irrigate are based on the recommended soil
moisture tension and the allowable depletion.
• Recommended soil moisture tension: Water stress in plants is related to soil
moisture tension. The higher the tension the greater the potential for water
stress. Research has determined the soil moisture tension at which irrigation
should occur. For example, some typical recommended values for citrus are 50-
70 kPa9, where it is recommended to use the larger values in cool, humid
conditions and the smaller values on warmer and dry conditions.
• Allowable depletion: Allowing a plant to deplete most of the available soil
moisture can reduce yields because of the excessive water stress. Thus, soil
moisture depletions are limited to those depletions that cost no yield lost
defined as the allowable depletion (frequently expressed as a percentage of the
available moisture). For example, for citrus the recommended allowable
depletion is 50% of the available soil moisture.10
j See Technical Brief on Irrigation Scheduling for further information.
Figure 5: Saturation, Field Capacity, and Permanent Wilting Point.
TB 5 – The Importance of Soil to water use
11
SECTION 8: HOW TO MEASURE SOIL MOISTURE?11
Measuring the soil moisture content allows monitoring the water available to the plant
for growth. When the water at any depth falls below the refill point or where there is no
remaining readily available water (RAW) then an irrigation event must be scheduled.
See Figure 4 in Section 4 to analyse when irrigation was conducted in that case.
Types of measuring equipment
There is a wide range of technical soil moisture monitoring equipment currently
available for farmers to use to help manage and monitor water use in the field. The
types of soil moisture monitoring equipment available can be divided into two
categories: soil suction measurement systems and soil moisture content measurement
systems.
a. Soil Suction Measurement Systems
Soil suction devices measure the (negative) pressure required by the plant to be able to
extract water from the soil. This force from the plant on the soil to draw the amount of
water it needs to grow can be measured as tension. The drier the soil, the more tightly
the water is held, and the more energy the plant has to use to extract the water from
the soil. Therefore devices that measure soil water potential are very good indicators of
the stress plants are under.
These devices enable farmers to keep crop stress to a minimum by managing irrigation
to ensure the correct soil water potential is maintained. In the case of water sensitive
crops, such as vegetables, a tension of –20 kPa is considered the refill point. The RAW is
the amount of water that is held between field capacity –8 kPa and –20 kPa. The devices
however, do not inform the farmer as to the volume of water that is required to be
applied.
• Tensiometers: A tensiometer is essentially a tube
filled with water that has a porous ceramic tip
which is buried in the soil at the depth which soil
moisture need to be measured. Tensiometers can
be buried at 2 to 3 different depths in the root
zone in order to obtain a soil moisture profile.
The water will move out to the drier soil until the
Figure 4
Figure 5
TB 5 – The Importance of Soil to water use
12
potential within the tensiometer is the same as that of the soil water. A vacuum
gauge records the level of suction required by the plant to draw water from the soil.
The vacuum gauge can be read manually by the farmer, but can also be measured
electronically and logged. See case study for an application.
• Resistance/Gypsum Blocks
Resistance blocks such as gypsum blocks are
made from a porous material with two electrodes
embedded in the material. They are buried in the
soil and they take on the soil water characteristics
of the surrounding soil, creating equilibrium. The
electrical resistance within the blocks is
measured. The electrical resistance of a block is
directly proportional to its water content, which
is related to the soil water potential of the soil surrounding the block.
• Wetting Front Detectors
Wetting front detectors are simple devices that are buried at points of interest and
provide information to farmers as to when water has reached that point in the soil
profile. When soil moisture increases above a set point the detector switches on, or
is activated, indicating that water has reached a given depth. When the soil moisture
dries to below a set point the detector switches off. Wetting front detectors are
often placed near the bottom of the root zone so that they can be used to warn
against over irrigation.
b. Soil Moisture Content Measurement Systems
Instruments that indirectly measure soil moisture content use sensors that are placed in
the soil at various depths in the root zone. The sensors measure properties that are
closely related to soil water content. Calibration equations can be used to convert the
property being measured by the sensor to soil water content.
• Capacitance - Frequency Domain Reflectometry devices (FDR)
FDR devices use the dielectric constant of the soil water media to calculate soil water
content. These types of instruments work on the basis that the dielectric of dry soil is
much lower than that of water. The soil dielectric is calculated by applying a voltage to
the plates and measuring the frequency.
TB 5 – The Importance of Soil to water use
13
• Time Domain Reflectometry devices (TDR)
TDR devices operate similarly to capacitance devices as they use the dielectric constant
of the soil water media to calculate soil water content. An electromagnetic signal is sent
down a steel probe which is buried in the soil at the desired depth. The signal reaches
the end of the probe and is reflected back to the control unit. The return time of the
signal varies with the soil dielectric constant and therefore relates to the water content
of the soil surrounding the probe.
• Neutron Probe
Neutron probes emit fast moving neutrons. When the neutrons collide with hydrogen in
the soil they are slowed and deflected. A detector on the probe counts returning slow
neutrons. The number of slow neutrons detected can be used to calculate soil water
content because changes in the amount of hydrogen in the soil between readings will
only come about from changes in water content. A wet soil will contain more hydrogen
than a dry soil and therefore more slow neutrons will be detected.
How to choose the right instrument?
Devices vary in their complexity, cost, accuracy and labour requirement for the
installation, monitoring and during the servicing. Individual requirements should be
indentified before purchasing a soil moisture monitoring device. As a minimum, a soil
moisture monitoring instrument needs to provide water content readings for the plant
root zone before and after irrigation and rainfall.
Before deciding on a soil moisture monitoring device farmers should consider the type
of information that the soil water monitoring device provides and the way how
information would be used, the labour intensity of the device and assess its labour
capacity, the suitability of the device for the farmers soil type/s and crop/s, the
investment and maintenance cost and the accuracy and repeatability of measurements.
TB 5 – The Importance of Soil to water use
14
Section 9: How to interpret soil moisture data?
Interpretation of soil moisture data is a key step on determining when to irrigate and
how much water to apply.
Interpretation of tensiometer data
The correct interpretation of tensiometer data is straightforward because it measures
the relative difficulty plants will be experiencing when their roots extract water from the
soil at a particular point in time. The table below provides some guidelines for
interpreting tensiometer readings. Soil type does not strictly affect interpretation, but
loam and clay soil types can hold a lot more available water than sandy soil, so the time
between irrigations and the critical reading of approximately 20 kPa indicating it is time
to irrigate will be greater in a clay soil than for sandy soils.k
Table 1: Critical soil tensiometer for vegetable crops12
Soil moisture
status
Tensiometer
reading kPa
Interpretation
Nearly saturated 0 Nearly saturated soil often occurs for a day or two following irrigation.
Danger of water-logged soils, a high water table, poor soil aeration, or the
tensiometer may have broken tension if readings persist.
Field capacity -10 Field capacity. Irrigations discontinued at field capacity to prevent waste by
deep percolation and leaching of nutrients below the root zone.
Irrigation range -20 Usual range for starting irrigations. Most of the available soil moisture is
used up in sandy loam soils. For clay loams, only one or two days of soil
moisture remain.
Dry -30 This is the stress range for most vegetable crops.
Extremely dry -80 Top range of accuracy of tensiometer. Readings above this are possible but
many tensiometers will break tension between 80 to 85 kPa.
Interpretation of capacitance data
Capacitance data is usually logged and then can be viewed using software supplied by
the manufacturers.
Soil moisture at individual sensors
k It is recommended to interpret tensiometer readings with a table supplied by the manufacturer or assess
it in relation to the soil profile in farm.
TB 5 – The Importance of Soil to water use
15
The data is collected from each sensor and graphed over time. The soil moisture data
can be collected at different depths in the soil profile. This type of data can be useful
because it shows where in the soil profile the water is being taken from. If water is being
extracted from deeper depths it means that the plant is working harder to get water
and it can mean that the plant is under water stress.
Total soil moisture for the depth being monitored
The moisture readings from each of the sensors can be added together to give the total
soil moisture for the depth of soil monitored. There are two key things to note from
figure 6 below, which is an example of a total soil profile graph.
First, the irrigations can be noticed by the vertical lines where water is added to the soil
by irrigation, or possibly a rainfall event. Second, the stairs pattern is explained as the
soil moisture is used by the plant.
TB 5 – The Importance of Soil to water use
16
SECTION 10: CASE STUDY
Managing soil for grown tomatoes in the Gascoyne River area13
Water is a limiting resource in Carnarvon, so efficient use of the water allocation for
vegetable crops is
essential. Knowing the
type of soil and measuring
the moisture in the soils
help farmers optimize
water use in tomatoes.
Tomatoes can use 70% of
the available soil moisture,
without suffering
significant yield loss. At
this point, the soil moisture tension in Gascoyne fine sandy loam is at 40kPal.
In Gascoyne sandy loam, this watering regime resulted in a total seasonal water
application between 350 and 450 mm (3500 to 4500 kL/ha), depending on the season
and the amount of water, stored in the soil before planting.
Tensiometers were installed at 30, 50 and 90cm depth and continuous recording
indicate the depth of the root system and the changing water demand, according to the
stage of the crop.
Initially, irrigation was scheduled using the tensiometer placed at 30 cm depth. When it
reads 40 to 45 kPa, farmers knew that the crop needed watering.
As the crop develops and roots grow deeper, water was withdrawn from around the
tensiometer at 50 cm depth. When this starts to happen, and the tensiometer read 40
to 45 kPa.
Having tensiometers placed at several depths allow farmers to adjust water run times
easier.
The key learning from this trial were that it was a good practice to allow one or two days
after irrigation for water infiltration, before checking tensiometer readings.
• If the tensiometer at 30 cm depth indicates falling soil moisture and the one at 50 cm
depth remains unchanged, increase the amount of water applied.
l 1Centibar = 1 kPa
Figure 6: Soil profilea
TB 5 – The Importance of Soil to water use
17
• If the tensiometer at 90 cm depth indicates rising soil moisture after irrigation, water
is draining below the root zone and being wasted. Decrease the amount of water
applied.
• If the tensiometer at 50 cm depth does not react, even after long water runs, a hard
pan is preventing the water from infiltrating and the site may be unsuitable for soil
moisture monitoring.
TB 5 – The Importance of Soil to water use
18
SECTION 11: REFERENCES AND FURTHER READINGS
Technical Papers
Building soils for better crops, sustainable soil management
http://www.sare.org/publications/bsbc/bsbc.pdf
A comprehensive guide on soil including soil properties and nutrient cycles.
Department of Agriculture WA: Irrigation
http://www.agric.wa.gov.au/search/search.cgi?collection=external&form=custom&met
a_y_and=0LWE0WATER0IRR0&sort=date
Contains fact sheets including information on soil moisture monitoring tools, irrigation
best management practices and irrigation systems.
Department of Primary Industries Queensland: Managing Water Resources
http://www.dpi.qld.gov.au/cps/rde/dpi/hs.xsl/4789_4346_ENA_HTML.htm
Information such as water balance scheduling and use of soil moisture monitoring tools.
Other Publications International Soil Moisture Equipment Comparison
http://www.cprl.ars.usda.gov/wmru/pdfs/WF-vol5-No2.pdf
Soil Water Monitoring with Inexpensive Equipment. 2000. By Richard Allen, University of
Idaho.
www.kimberly.uidaho.edu/water/swm
Tensiometer Use in Irrigation Scheduling. 1997. By Mahbub Alam and Danny H. Rogers.
Kansas State University Agricultural Experiment Station and Cooperative Extension
Service, Manhattan, KS. 6 p.
www.oznet.ksu.edu/library/ageng2/l796.pdf.
Measuring Soil Moisture. 1998. By Blaine Hanson and Steve Orloff. University of California,
Davis, CA. 34 p.
http://gwpa.uckac.edu/pdf/direct_soil_mositure_measurement.pdf.
TB 5 – The Importance of Soil to water use
19
Soil Texturing
http://www.agric.wa.gov.au/objtwr/imported_assets/content/lwe/water/irr/asoiltextur
ingsmall.pdf
This fact sheet provides useful on how farmers can distinguish soil texture.
Web Sites Calculating Readily Available Water
http://www.agric.wa.gov.au/objtwr/imported_assets/content/lwe/water/irr/rawrh.pdf
This fact sheet provides useful information on how to calculate Readily Available water
The Soil Water Content Sensor discussion group
http://www.horticulture.com.au/
An Internet search under "soil moisture monitoring" (or similar key words) will yield
hundreds of additional Web sites offering products, reviews, and guidelines.
Vegetables WA: Efficient Irrigation of vegetables on sands
http://www.vegetableswa.com.au/ Information on good irrigation management; soil
moisture monitoring in sand; and calculating water requirements.
Soil
http://www.cprl.ars.usda.gov/wmru/pdfs/C2_Irrigation%20Monograph%2030.pdf
Soil Moisture Monitoring: Low-Cost Tools and Methods
http://attra.ncat.org/attra-pub/PDF/soil_moisture.pdf
Soil Water and Monitoring Technology
http://www.cprl.ars.usda.gov/wmru/pdfs/C2_Irrigation%20Monograph%2030.pdf
Soil Health Knowledge Bank
http://soilhealthknowledge.com.au/
This site provide an overview of current soil health knowledge and tools to assess soil
condition providing information on soil properties, processes and management for
profit across a range of industries and regions of Australia.
Soil types
http://websoilsurvey.nrcs.usda.gov/app/
TB 5 – The Importance of Soil to water use
20
This website provide information on soil types throughout USA
Tools and systems for assessing soil health
http://www.dpi.vic.gov.au/dpi/vro/vrosite.nsf/pages/soil_health_tools_1
Soil Health Knowledge Bank in Australia
soilhealthknowledge.com.au
1 For more information on soil texture. See http://www.agric.wa.gov.au/objtwr/imported_assets/content/lwe/water/irr/rawrh.pdf 2 http://www.extension.umn.edu/distribution/cropsystems/components/3115s01.html 3 http://www.fao.org/ag/ca/doc/Soil_compaction.pdf 4 http://epa.gov/nps/agmm/chap4c.pdf 5 http://www.fao.org/docrep/r4082e/r4082e03.htm#2.5.3 capillary rise 6 http://www.horticulture.com.au/librarymanager/libs/165/Managing_Water_Yield_Profit.pdf 7 http://www.hbrc.govt.nz/WhatWeDo/Climate/SoilMoisture/tabid/1046/Default.aspx 8 For more information see http://www.agric.wa.gov.au/objtwr/imported_assets/content/lwe/water/irr/rawrh.pdf 9 http://www.specmeters.com/pdf/6450WD.pdf. 10 Blaine Hanson and Larry Schwankl On-Farm Irrigation. Scheduling Irrigations: When and How Much Water to Apply. University of California. 2007 11 http://www.horticulture.com.au/librarymanager/libs/165/Managing_Water_Yield_Profit.pdf 12 (Source: www.horticulture.au) 13 http://www.agric.wa.gov.au/objtwr/imported_assets/content/lwe/water/irr/fn027_1990.pdf